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Sepra work alongside different Small & Large Mineral deposit mines and processing units across India and offer financial investment, joint ventures and risk management tools.

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Talc (Soap Stone)

Talc, or talcum, is a clay mineral, Talc dominantly forms from the metamorphism of magnesian minerals such as serpentine, pyroxene, amphibole, and olivine, in the presence of carbon dioxide and water. This is known as "talc carbonation" or "steatization" and produces a suite of rocks known as talc carbonates.

Talc is primarily formed by hydration and carbonation by this reaction:


dolomite 3CaMg(CO3)2 + silica 4SiO2 + waterH2O → talc Mg3Si4O10(OH)2 + calcite 3CaCO3 + carbon dioxide 3CO2

Talc can also be formed via a reaction between dolomite and silica, which is typical of skarnification of dolomites by silica-flooding in contact metamorphic aureoles:

dolomite 3CaMg(CO3)2 + silica 4SiO2 + waterH2O → talc Mg3Si4O10(OH)2 + calcite 3CaCO3 + carbon dioxide 3CO2

Product Variants :

Grade A Grade B Grade C Grade D Grade E
Brightness >90% Brightness 85%-90% Brightness 80%-85% Brightness 75%-80% Brightness 70%-75%
CaO levels
<10%
CaO levels
<5%
CaO levels
<3%
CaO levels
<2%
CaO levels
<2%

Basic Chemical Analysis :

Sr. No Parameters Talc Grade
1 MgO 29.5%
2 SiO 2 61.5%
3 Fe 2O 3 2.56%
4 CaO 0.56%
5 Soluble Salts 0.55%
6 Al 2O 3 0.55%
6 PH(at 10%) 8.5 - 9.5


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